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Chiral biomarkers and microfossils in carbonaceous meteorites

机译:碳质陨石中的手性生物标志物和微化石

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Homochirality of the biomolecules (D-sugars of DNA and RNA and L-amino acids of proteins) is a fundamental property of all life on Earth. Abiotic mechanisms yield racemic mixtures (D/L=l) of chiral molecules and after the death of an organism, the enantiopure chiral biomolecules slowly racemize. Several independent investigators have now established that the amino acids present in CI1 and CM2 carbonaceous meteorites have a moderate to strong excess of the L-enantiomer. Stable isotope data have established that these amino acids are both indigenous and extraterrestrial. Carbonaceous meteorites also contain many other strong chemical biomarkers including purines and pyrimidines (nitrogen heterocycles of nucleic acids); pristine and phytane (components of the chlorophyll pigment) and morphological biomarkers (microfossils of filamentous cyanobacteria). Energy dispersive X-ray Spectroscopy (EDS) analysis reveals that nitrogen is below the detectability level in most of the meteorite filaments as well as in Cambrian Trilobites and filaments of 2.7 Gya Archaean cyanobacteria from Karelia. The deficiency of nitrogen in the filaments and the total absence of sugars, of twelve of the life-critical protein amino acids, and two of the nucleobases of DNA and RNA provide clear and convincing evidence that these filaments are not modern biological contaminants. This paper reviews the chiral, chemical biomarkers morphological biomarkers and microfossils in carbonaceous meteorites. This paper reviews chiral and morphological biomarkers and discusses the missing nitrogen, sugars, protein amino acids, and nucleobases as "bio-discriminators" that exclude modern biological contaminants as a possible explanation for the permineralized cyanobacterial filaments found in the meteorites.
机译:生物分子(DNA和RNA的D型糖和蛋白质的L型氨基酸)的同质性是地球上所有生命的基本特征。非生物机制产生手性分子的外消旋混合物(D / L = 1),并且在生物死亡后,对映纯手性生物分子缓慢消旋。几位独立研究者现已确定,存在于CI1和CM2碳质陨石中的氨基酸比L-对映异构体有中等至强烈过量。稳定的同位素数据已确定这些氨基酸既是天然的,也是外星的。碳质陨石还包含许多其他强大的化学生物标记,包括嘌呤和嘧啶(核酸的氮杂环);原始和植烷(叶绿素色素的成分)和形态生物标志物(丝状蓝细菌的微化石)。能量色散X射线光谱(EDS)分析表明,在大多数陨石丝以及寒武纪三叶虫和卡累利阿州2.7 Gya古细菌蓝藻细菌丝中,氮均低于可检测水平。细丝中氮的缺乏和糖的缺失,其中12种对生命至关重要的蛋白质氨基酸以及DNA和RNA的两个核碱基均提供了明确而令人信服的证据,证明这些细丝不是现代生物污染物。本文综述了碳质陨石中的手性,化学生物标志物,形态生物标志物和微化石。本文综述了手性和形态生物标志物,并讨论了缺失的氮,糖,蛋白质氨基酸和核碱基作为“生物标志物”,它们排除了现代生物污染物,从而解释了陨石中矿化的蓝细菌细丝。

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